For more than two decades, scientists
studying hydrothermal circulation in the water under the seafloor have assumed that the flow is relatively stable.
Not exact matches
«
Hydrothermal siphon» drives water
circulation through seafloor: New
study explains previous observations of ocean water flowing through the seafloor from one seamount to another.»
The new
study determined that the methane contained in the fluid leached from sub-seafloor rocks, and was not formed through
hydrothermal vent
circulation, as had been previously thought.